Title: Hydrologic Cycle/Water Balances
1Hydrologic Cycle/Water Balances
2Earths Water
- Covers approximately 75 of the surface
- Volcanic emissions
- Only known substance that naturally exists as a
gas, liquid, and solid at surface temperatures
and pressures
http//earthobservatory.nasa.gov/Library/Water/
3One estimate of global water distribution
http//earthobservatory.nasa.gov/Library/Water/
4Fresh Water
5Hydrologic Cycle
- Powered by energy from the sun
- Evaporation 90 of atmospheric water
- Transpiration 10
- Evaporation exceeds precipitation over oceans
- Precipitation exceeds evaporation over continents
- All water stored in atmosphere would cover
surface to a depth of 2.5 centimeters - 1 m average annual precipitation
http//earthobservatory.nasa.gov/Library/Water/
6Hydrologic Cycle
In the hydrologic cycle, individual water
molecules travel between the oceans, water vapor
in the atmosphere, water and ice on the land, and
underground water. (Image by Hailey King, NASA
GSFC.)
http//earthobservatory.nasa.gov/Library/Water/
7Florida
8Florida
9U.S. total, surface-water, and ground-water
withdrawals, 2000
http//water.usgs.gov/pubs/circ/ 2004/circ1268/htd
ocs/text-total.html
10U.S. total water withdrawals by category, 2000
http//water.usgs.gov/pubs/circ/2004/circ1268/htdo
cs/text-total.html
11Trends in population and freshwater withdrawals
by source, 1950-2000
http//water.usgs.gov/pubs/circ/2004/circ1268/htdo
cs/text-total.html
12Water (Mass) Balance
- In Out Change in Storage
- Totally general
- Usually for a particular time interval
- Many ways to break up components
- Different reservoirs can be considered
13Water (Mass) Balance
- Principal components
- Precipitation
- Evaporation
- Transpiration
- Runoff
- P E T Ro Change in Storage
- Units?
14Ground Water (Mass) Balance
- Principal components
- Recharge
- Inflow
- Transpiration
- Outflow
- R Qin T Qout Change in Storage